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The Main Kopeh Dagh Fault in Turkmenistan is more than impressive. It’s a NW-SE trending right-lateral strike-slip fault with a wonderful morphological expression that can be traced for several hundreds of kilometres. This fault marks the northernmost deformation front of...

One focus of EwF is to investigate the active faults in the Tien Shan. We map them from satellite data and in the field, we measure their slip rates, and we reconstruct their earthquake history. These studies help us to understand how the continents deform. The data we gather can...

By Dr John Elliott, project partner and Post-Doctoral Research Associate at COMET+, Department of Earth Sciences, University of Oxford This article was first published in the Blue Marble,The magazine of the UK’s National Centre for Earth Observation, in Winter 2011. Almost two...